Biomarker distribution of sediment core PS93/006-1 ...

The northeastern Fram Strait at the entrance to the Arctic Ocean represents a key observatory for sea ice reconstructions as it sensitively reacts to environmental changes. A combined biomarker approach (HBIs, sterols, alkenones) was carried out on Core PS93/006-1 from the western Svalbard margin to...

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Main Authors: Stein, Ruediger, Kremer, Anne, Fahl, Kirsten
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.884799
https://doi.pangaea.de/10.1594/PANGAEA.884799
id ftdatacite:10.1594/pangaea.884799
record_format openpolar
spelling ftdatacite:10.1594/pangaea.884799 2024-09-15T17:53:56+00:00 Biomarker distribution of sediment core PS93/006-1 ... Stein, Ruediger Kremer, Anne Fahl, Kirsten 2018 application/zip https://dx.doi.org/10.1594/pangaea.884799 https://doi.pangaea.de/10.1594/PANGAEA.884799 en eng PANGAEA https://dx.doi.org/10.1007/s41063-018-0052-0 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Kasten corer PS93.1 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2018 ftdatacite https://doi.org/10.1594/pangaea.88479910.1007/s41063-018-0052-0 2024-07-03T13:15:54Z The northeastern Fram Strait at the entrance to the Arctic Ocean represents a key observatory for sea ice reconstructions as it sensitively reacts to environmental changes. A combined biomarker approach (HBIs, sterols, alkenones) was carried out on Core PS93/006-1 from the western Svalbard margin to reconstruct sea ice conditions related to glacial-interglacial cycles of the last 190 ka. The continuous presence of sea ice demonstrates the strong influence of the East Greenland Current in the eastern Fram Strait. Glacial intervals are characterised by extended sea ice conditions with perennial sea ice cover during early MIS 6, the Penultimate Glacial Maximum, the interstadial MIS 5d, MIS 4 and the Last Glacial Maximum. Less severe, yet highly variable, sea ice conditions with more frequent summer melt dominated the interglacial stages. By comparison with previous sea ice reconstructions along the western and northern continental margin of Svalbard, the highly variable impact of different environmental forces ... : Supplement to: Kremer, Anne; Stein, Ruediger; Fahl, Kirsten; Bauch, Henning A; Mackensen, Andreas; Niessen, Frank (2018): A 190-ka biomarker record revealing interactions between sea ice, Atlantic Water inflow and ice sheet activity in eastern Fram Strait. arktos - The Journal of Arctic Geosciences, 4(1) ... Article in Journal/Newspaper Arctic Ocean East Greenland east greenland current Fram Strait Greenland Ice Sheet Sea ice Svalbard Svalbard margin DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Kasten corer
PS93.1
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Kasten corer
PS93.1
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Stein, Ruediger
Kremer, Anne
Fahl, Kirsten
Biomarker distribution of sediment core PS93/006-1 ...
topic_facet Kasten corer
PS93.1
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The northeastern Fram Strait at the entrance to the Arctic Ocean represents a key observatory for sea ice reconstructions as it sensitively reacts to environmental changes. A combined biomarker approach (HBIs, sterols, alkenones) was carried out on Core PS93/006-1 from the western Svalbard margin to reconstruct sea ice conditions related to glacial-interglacial cycles of the last 190 ka. The continuous presence of sea ice demonstrates the strong influence of the East Greenland Current in the eastern Fram Strait. Glacial intervals are characterised by extended sea ice conditions with perennial sea ice cover during early MIS 6, the Penultimate Glacial Maximum, the interstadial MIS 5d, MIS 4 and the Last Glacial Maximum. Less severe, yet highly variable, sea ice conditions with more frequent summer melt dominated the interglacial stages. By comparison with previous sea ice reconstructions along the western and northern continental margin of Svalbard, the highly variable impact of different environmental forces ... : Supplement to: Kremer, Anne; Stein, Ruediger; Fahl, Kirsten; Bauch, Henning A; Mackensen, Andreas; Niessen, Frank (2018): A 190-ka biomarker record revealing interactions between sea ice, Atlantic Water inflow and ice sheet activity in eastern Fram Strait. arktos - The Journal of Arctic Geosciences, 4(1) ...
format Article in Journal/Newspaper
author Stein, Ruediger
Kremer, Anne
Fahl, Kirsten
author_facet Stein, Ruediger
Kremer, Anne
Fahl, Kirsten
author_sort Stein, Ruediger
title Biomarker distribution of sediment core PS93/006-1 ...
title_short Biomarker distribution of sediment core PS93/006-1 ...
title_full Biomarker distribution of sediment core PS93/006-1 ...
title_fullStr Biomarker distribution of sediment core PS93/006-1 ...
title_full_unstemmed Biomarker distribution of sediment core PS93/006-1 ...
title_sort biomarker distribution of sediment core ps93/006-1 ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.884799
https://doi.pangaea.de/10.1594/PANGAEA.884799
genre Arctic Ocean
East Greenland
east greenland current
Fram Strait
Greenland
Ice Sheet
Sea ice
Svalbard
Svalbard margin
genre_facet Arctic Ocean
East Greenland
east greenland current
Fram Strait
Greenland
Ice Sheet
Sea ice
Svalbard
Svalbard margin
op_relation https://dx.doi.org/10.1007/s41063-018-0052-0
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.88479910.1007/s41063-018-0052-0
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